Single repeated contact ice charging

Charge transfer in single, repeated collision of ice surfaces. An experimental study of the charging of colliding ice surfaces replicates in part a study (Mason & Dash, 2000, https://doi.org/10.1029/2000JD900104) in which there was qualitative agreement with a prediction of Baker and Dash, (1989...

Full description

Bibliographic Details
Main Author: Turner, Gary
Format: Dataset
Language:unknown
Published: Mendeley 2020
Subjects:
Ice
Online Access:https://dx.doi.org/10.17632/gp5g66btpr.1
https://data.mendeley.com/datasets/gp5g66btpr/1
id ftdatacite:10.17632/gp5g66btpr.1
record_format openpolar
spelling ftdatacite:10.17632/gp5g66btpr.1 2023-05-15T16:41:22+02:00 Single repeated contact ice charging Turner, Gary 2020 https://dx.doi.org/10.17632/gp5g66btpr.1 https://data.mendeley.com/datasets/gp5g66btpr/1 unknown Mendeley https://dx.doi.org/10.17632/gp5g66btpr Creative Commons Attribution 4.0 International info:eu-repo/semantics/openAccess https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 CC-BY Charge Transfer Atmospheric Electricity Ice dataset Dataset 2020 ftdatacite https://doi.org/10.17632/gp5g66btpr.1 https://doi.org/10.17632/gp5g66btpr 2021-11-05T12:55:41Z Charge transfer in single, repeated collision of ice surfaces. An experimental study of the charging of colliding ice surfaces replicates in part a study (Mason & Dash, 2000, https://doi.org/10.1029/2000JD900104) in which there was qualitative agreement with a prediction of Baker and Dash, (1989, https://doi.org/10.1016/0022-0248(89)90581-2 1994, https://doi.org/10.1029/93JD01633) based on the proposal by Turner and Stow (1984, https://doi.org/10.1080/01418618408236549). However, the magnitude (a few picoCoulombs) of the transferred charge observed by Mason and Dash (2000) was considerably greater, raising doubt that the mechanism of charge transfer is solely a surface-layer effect. The current study examined charge transfer in single collisions between an ice pellet and an ice sheet (instead of two flat surfaces) and its dependence on the common temperature, saturation and environmental pressure. The polarity was consistent with the earlier results in that the more-rapidly growing particle charged positively. The magnitude (also a few picoCoulombs) of the charge transferred increased slightly over an even greater range of temperature (235K to 268K). The sign of the charge transfer is explicable in terms of the relative growth-rate of the contacting surfaces. This result (with surfaces at a common temperature) provides quantitative confirmation of that earlier work (where temperature differentials existed) without the need for postulating (Dash et al, 2001, https://doi.org/10.1029/2001JD900109) collisional melting. It is inferred that the charge is carried in mass transferred between the colliding surfaces, supporting the conjecture by Dash et al (2006, https://doi.org/10.1103/RevModPhys.78.695) that the mass transfer can be driven by differences in curvature, and contradicting the proposition by Baker and Nelson (2002, https://doi.org/10.1016/S1631-0705(02)01408-1) that the transfer between different shapes would be driven from sharp to flat surfaces. Dataset Ice Sheet DataCite Metadata Store (German National Library of Science and Technology)
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language unknown
topic Charge Transfer
Atmospheric Electricity
Ice
spellingShingle Charge Transfer
Atmospheric Electricity
Ice
Turner, Gary
Single repeated contact ice charging
topic_facet Charge Transfer
Atmospheric Electricity
Ice
description Charge transfer in single, repeated collision of ice surfaces. An experimental study of the charging of colliding ice surfaces replicates in part a study (Mason & Dash, 2000, https://doi.org/10.1029/2000JD900104) in which there was qualitative agreement with a prediction of Baker and Dash, (1989, https://doi.org/10.1016/0022-0248(89)90581-2 1994, https://doi.org/10.1029/93JD01633) based on the proposal by Turner and Stow (1984, https://doi.org/10.1080/01418618408236549). However, the magnitude (a few picoCoulombs) of the transferred charge observed by Mason and Dash (2000) was considerably greater, raising doubt that the mechanism of charge transfer is solely a surface-layer effect. The current study examined charge transfer in single collisions between an ice pellet and an ice sheet (instead of two flat surfaces) and its dependence on the common temperature, saturation and environmental pressure. The polarity was consistent with the earlier results in that the more-rapidly growing particle charged positively. The magnitude (also a few picoCoulombs) of the charge transferred increased slightly over an even greater range of temperature (235K to 268K). The sign of the charge transfer is explicable in terms of the relative growth-rate of the contacting surfaces. This result (with surfaces at a common temperature) provides quantitative confirmation of that earlier work (where temperature differentials existed) without the need for postulating (Dash et al, 2001, https://doi.org/10.1029/2001JD900109) collisional melting. It is inferred that the charge is carried in mass transferred between the colliding surfaces, supporting the conjecture by Dash et al (2006, https://doi.org/10.1103/RevModPhys.78.695) that the mass transfer can be driven by differences in curvature, and contradicting the proposition by Baker and Nelson (2002, https://doi.org/10.1016/S1631-0705(02)01408-1) that the transfer between different shapes would be driven from sharp to flat surfaces.
format Dataset
author Turner, Gary
author_facet Turner, Gary
author_sort Turner, Gary
title Single repeated contact ice charging
title_short Single repeated contact ice charging
title_full Single repeated contact ice charging
title_fullStr Single repeated contact ice charging
title_full_unstemmed Single repeated contact ice charging
title_sort single repeated contact ice charging
publisher Mendeley
publishDate 2020
url https://dx.doi.org/10.17632/gp5g66btpr.1
https://data.mendeley.com/datasets/gp5g66btpr/1
genre Ice Sheet
genre_facet Ice Sheet
op_relation https://dx.doi.org/10.17632/gp5g66btpr
op_rights Creative Commons Attribution 4.0 International
info:eu-repo/semantics/openAccess
https://creativecommons.org/licenses/by/4.0/legalcode
cc-by-4.0
op_rightsnorm CC-BY
op_doi https://doi.org/10.17632/gp5g66btpr.1
https://doi.org/10.17632/gp5g66btpr
_version_ 1766031792723197952